Vertical structure of recent Arctic warming
By Rune Graversen, T. Mauritsen, M. Tjernström, E. Källén, G. Svensson. Nature, 2008
613 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/9a1567b144daefefb959546386b4237e9c1e7c0f
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
In Global and Planetary Change
Citations in the corpus
- Seasonality of polar surface warming amplification in climate simulations (2009, result): “Figure 2c and the results from other CMIP3 models (not shown) suggest that the vertical structure of Arctic warming in summer in climate simulations is qualitatively consistent 2 of 6 with the results obtained from the reanalysis data [Graversen et al., 2008].”
- Impacts of climate change on the seasonal distribution of migratory caribou (2009, background): “Arctic ecosystems are especially vulnerable to global warming as polar regions are expected to exhibit the greatest degree of change (ACIA, 2004; Graverson et al., 2008).”
- The Arctic Summer Cloud Ocean Study (ASCOS): Overview and experimental design (2013, background): “In summer the presence of melting snow and ice at the surface effectively limits near-surface warming above the melting point, although some studies indicate warming aloft (Graversen et al., 2008); in areas where ice completely melts away, however, substantial surface warming occurs.”
- Surface radiation climatology for Ny-Ålesund, Svalbard (78.9° N), basic observations for trend detection (2015, background): “Also changes in atmospheric circulation and the related increase in meridional heat transport to the high latitudes account for Arctic warming (Graversen et al. 2008; Zhang et al. 2008), as well as the possibility that Arctic atmospheric circulation itself is modified by the strong warming (Francis…”
- Ice structures, patterns, and processes: A view across the icefields (2012, background): “Classically, polar amplification of climate change is understood to be caused by the positive feedback mechanism of snow and sea-ice changes, but changes in the atmospheric meridional transport of heat and moisture are also very significant driving factors (Graversen et al., 2008).”
- Arctic amplification enhanced by latent energy transport of atmospheric planetary waves (2016, background): “142: 2046–2054 (2016) Atmospheric Energy Transport to the Arctic 2053 current observations (Graversen et al., 2008; Serreze and Barry, 2011; Cohen et al., 2014), and climate models (Manabe and Bryan, 1985; Collins et al., 2013).”
- The central role of diminishing sea ice in recent Arctic temperature amplification (2010, methodology): “Furthermore, we build on the results of Graversen et al.8 by including the post-2001 period, during which time sea ice retreat has accelerated5,7.”
- Exposure and effects assessment of persistent organohalogen contaminants in arctic wildlife and fish. (2010, background): “An intensely focused environmental stress element in the Arctic is climate change caused by global warming and/or temperature changes (Graversen et al., 2008).”
- Reanalyses Suitable for Characterizing Long-Term Trends (2010, background): “…applications (e.g., Simmons et al. 2004, 2009), but great care must be taken, care that cannot be assumed of end users, occasionally resulting in high-profile findings upon which considerable doubt has been cast (e.g., Graversen et al. 2008; Thorne 2008; Grant et al. 2008; Bitz and Fu 2008).”
- Climatological Characteristics of Arctic and Antarctic Surface-Based Inversions* (2011, methodology): “The results for stations in Alaska are in very good agreement with those of Bourne et al. (2010), who also used IGRA data to study SBI characteristics in that region of the Arctic, which instills confidence in the reproducibility of these and other climatological statistics presented here.”